The Geomorphic Cycle

The Geomorphic Cycle, also known as the cycle of erosion, describes how landscapes evolve over time. It starts with the uplift of land, creating mountains. Weathering and erosion gradually wear down these mountains, transporting sediment to valleys and riverbeds. As rivers flow, they sculpt the land, forming features like canyons and floodplains. Eventually, sediment is deposited in deltas and coastal areas. This cycle is continuous, as rising land and changing climates can restart the process, shaping our planet’s surface over millions of years. Understanding this cycle helps us comprehend landforms and geological changes.